fault lines
convergent plate boundaries
"plates" are the term for the giant sheets of rock on the earths crust
Tectonic plate boundaries are specific areas where the Earth's plates interact and move against each other, leading to seismic activity such as earthquakes. These boundaries can be categorized into different types based on the direction of the plate movement, such as convergent, divergent, and transform boundaries.
fault lines
The edges of continental plates are called fault lines because they are boundaries where tectonic plates meet and interact. These interactions can create faults, which are fractures within the Earth's crust where rocks have moved relative to each other. Fault lines are prone to seismic activity such as earthquakes due to the stress and movement along these boundaries.
QuestionThe term for the circular movement of material inside earth's mantle is convection current. This current causes the movement of the tectonic plates.
QuestionThe term for the circular movement of material inside earth's mantle is convection current. This current causes the movement of the tectonic plates.
QuestionThe term for the circular movement of material inside earth's mantle is convection current. This current causes the movement of the tectonic plates.
QuestionThe term for the circular movement of material inside earth's mantle is convection current. This current causes the movement of the tectonic plates.
The term that refers to the several large sections into which the lithosphere is broken is "tectonic plates." These plates float on the semi-fluid asthenosphere beneath them and interact at their boundaries, leading to geological phenomena such as earthquakes, volcanic activity, and the formation of mountains.
The term is "orogenesis." It refers to the geological process of mountain building, typically occurring at convergent plate boundaries where tectonic plates collide, leading to the uplift of the Earth's crust and the formation of mountain ranges.
A rift boundary is a divergent boundary, where two plates of the earth's crust are moving away from each other. Divergent boundaries occur at mid-oceanic ridges on the sea floor, but usually the term rift is used to describe divergent boundaries on the land. The best known one is in eastern Africa.